ALMA 873 $μ$m Polarization Observations of the PDS~70 Disk
Hauyu Baobab Liu, Kiyoaki Doi, Simon Casassus, Akimasa Kataoka, Ruobing Dong, Jun Hashimoto, Philipp Weber
TL;DR
This paper presents deep ALMA 873\,μm full-polarization observations of the PDS 70 protoplanetary disk, a system with two confirmed accreting planets, to constrain dust grain growth via self-scattering. By combining Band 7 polarization with multi-band continuum data and performing Monte Carlo radiative transfer modeling, the authors infer a maximum dust grain size of roughly $a_{\rm max} \approx (70-90)\,\mu$m in the rings and crescents, and a marginally optically thick ring on scales $\gtrsim$10 AU. The polarization patterns, together with azimuthal variations in the spectral index $\alpha_{\rm b6-b7}$, support a fragmentation-limited growth scenario with fragmentation velocity $v_{\rm frag}$ of order $1\,\rm m\,s^{-1}$ outside the water snowline. This suggests that stickiness due to ice coatings is insufficient to grow grains beyond $\sim$100\,μm in these regions, highlighting fragmentation or bouncing as key barriers in the natal disk environment that forms planets, with future multi-frequency polarization offering a decisive test of the model.
Abstract
At a 112.4 pc distance, the PDS70 protoplanetary disk is a rare case that has been confirmed to host two accreting planets. This makes it the most important laboratory for studying dust growth in the context of planet formation. Here we present the first deep, full polarization observations at 873 $μ$m wavelength. We detected $\sim$1%-2.5% linear polarization over the bulk of the $\sim$55-100 AU (sub)millimeter ring. The polarization position angles align preferentially with the projected minor axis of the disk. The standard interpretation is that the observed polarization is caused by dust self-scattering, with a maximum dust grain size of $\sim$100 $μ$m. On $\gtrsim$10 AU scales, which can be resolved by the presented 873-3075 $μ$m observations, the ring is marginally optical thick at 873 $μ$m wavelength. Using Monte Carlo radiative transfer simulations, we found that an azimuthally asymmetric, marginally optically thick ring with a maximum dust grain size of $\sim$87 $μ$m can reproduce the observed 873 $μ$m polarization position angles and percentages. This study indicates that the coagulation of ice-coated dust in the protoplanetary disk may be limited by fragmentation or bouncing.
